'Saturated parcel' diaporamas de présentation

Convection and Atmospheric Stability

Convection and Atmospheric Stability . AOS 101 Dis. 305. Atmospheric Stability. What is stability? Stability refers to a condition of equilibrium If we apply some perturbation to a system, how will that system be affected? Stable: System returns to original state

796 views • 53 slides

Lecture 8

Lecture 8. Saturated Adiabatic Processes. Liquid. Phase Changes. condensation. Gas (Vapor). evaporation. melting. deposition. sublimation. freezing. Solid (Ice). Energy absorbed. Energy released. Latent Heat . Heat released or absorbed during a phase change of water AMS Glossary.

441 views • 34 slides

Adiabatic Processes

Adiabatic Processes. Created By: Mr. Kreeger. Homework and Page References. Textbook-Page 484, Review Book-Page 576 HW #1- Explain why there is a difference between the dry adiabatic lapse rate and the moist adiabatic lapse rate. Explain the conditions responsible for Absolute stability

426 views • 15 slides

Lecture 12: Atmospheric moisture (Ch 5)

148 views • 14 slides

The tephigram

The tephigram. Allows a radiosonde profile to be analysed for stability Allows calculations involving moisture content (e.g. saturated adiabatic lapse rate) to be performed graphically Is very confusing at first sight!. Basic idea. Plot temperature as x-axis and entropy as y

634 views • 8 slides

The tephigram

The tephigram. Allows a radiosonde profile to be analysed for stability Allows calculations involving moisture content (e.g. saturated adiabatic lapse rate) to be performed graphically Is very confusing at first sight!. Basic idea. Plot temperature as x-axis and entropy as y

410 views • 8 slides